Official Series Description


Lab Data Summary

Aggregate lab data for the HUGGINS soil series. This aggregation is based on all pedons with a current taxon name of HUGGINS, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to HUGGINS were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
6440A2494S1958SD095005HUGGINS5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4108315,-101.1988907
6440A2498S1958SD095010HUGGINS5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5611115,-101.1277771

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HUGGINS soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the HUGGINS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the HUGGINS series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the HUGGINS series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D mountains figure.

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Competing Series

Soil series competing with HUGGINS share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the HUGGINS series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the HUGGINS series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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Soil series sharing subgroup-level classification with HUGGINS, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. SD-2012-03-15-97 | Todd County - April 1974

    Typical pattern of soils in association 2 (Soil Survey of Todd County, SD; 1974).

Map Units

Map units containing HUGGINS as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Huggins-Epping silt loams, 5 to 15 percent slopesHpD14220353373cvq4sd09519711:20000
Huggins-Kadoka silt loams, 2 to 5 percent slopesHuB7517353375cvq6sd09519711:20000
Epping-Huggins silt loams, 15 to 40 percent slopesEhE4136353363cvptsd09519711:20000
Huggins silt loam, 5 to 9 percent slopesHnC2423353372cvq3sd09519711:20000
Epping-Huggins silt loams, 5 to 15 percent slopesEhD2256353362cvpssd09519711:20000
Huggins silt loam, 2 to 5 percent slopesHnB1976353371cvq2sd09519711:20000
Huggins and Wortman silt loams, 2 to 5 percent slopesHwB1399353376cvq7sd09519711:20000
Huggins-Kadoka silt loams, 0 to 2 percent slopesHuA768353374cvq5sd09519711:20000
Kadoka-Huggins silt loams, 2 to 5 percent slopesKdB11708353003cvb6sd12119671:31680
Huggins-Kadoka silt loams, 2 to 9 percent slopesHwB11547352998cvb1sd12119671:31680
Huggins silt loam, 0 to 2 percent slopesHuA9426352997cvb0sd12119671:31680
Kadoka-Huggins silt loams, 5 to 9 percent slopesKdC8270353004cvb7sd12119671:31680
Huggins-Kadoka silt loams, 3 to 9 percent slopesHkB3696354397cws5sd12319751:20000
Huggins silt loam, 0 to 3 percent slopesHgA1756354396cws4sd12319751:20000
Kadoka-Huggins silt loams, 3 to 9 percent slopesKdC78382925503cv5tsd61019651:20000
Huggins silt loam, 0 to 3 percent slopesHwA10392925514cv5nsd61019651:20000

Map of Series Extent

Approximate geographic distribution of the HUGGINS soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .